The topography and geology of the Fayum province of Egypt — John Shaqi
The topography and geology of the Fayum province of EgyptBeadnell, H. J. L. (Hugh John Llewellyn)
Science
The topography and geology of the Fayum province of Egypt
Beadnell, H. J. L. (Hugh John Llewellyn)
Geology -- Egypt
In 1882, as a counter-project to other irrigation schemes, Cope
Whitehouse suggested[17] utilising as a reservoir the Wadi Rayan,
a depression which had been referred to by Linant de Bellefonds.[18]
At the request of Sir Colin Scott Moncrieff the Government deputed
Colonel Western to make plans of the Wadi Rayan and surrounding country
and to ascertain the capacity of the depression and its capability
of being used as a reservoir. Liernur Bey under his direction
prepared a contoured map, and Colonel Western’s report, plans, and
estimates were published.[19] Some general details of the wadi and
surrounding hills are given and the detailed survey showed that the
30 metre contour line (above sea-level) enclosed an area of 706 square
kilometres (170,000 feddans). The lowest points of the depression were
found at 42 metres below sea-level. The sand, scrub and springs are
briefly referred to and the discharge of the latter is given as equal
to that of a very slow-going four inch hand pipe, the water running
out at about + 20 m. and disappearing in the sand. Wadi Muêla was
found to be separated from the Rayan depression by sandhills and rock
at a mean level of + 50 metres, the lowest point in Muêla being at +
25 metres. A line of levels was run from Rayan through Muêla to the
Nile Valley, the highest point crossed being at + 105 metres; for
fifteen kilometres the level was not below + 75 metres. In order to
find the most suitable passage for a canal to connect the Nile with
the Wadi Rayan two lines of level were made after a reconnaissance of
the hills near Sidmant el Jebel: the southern, from Ezba Menesi Ali,
near the Gharaq canal, to Mazana on the Bahr Yusef, being considered
the best. Along this line the highest point was only at + 44·7 metres
and the average + 35 metres along four kilometres. Borings were not
made here but judging from the surface excavation would be mostly
in soft limestone, sand, and conglomerate. A much shorter route is
from Deshasleh on the Bahr Yusef over the hills about 5 kilometres
to the south of Mazana or Sidmant into the Wadi Gharaq, a distance
of 30 kilometres. This route was not however levelled but is fairly
straight and apparently not much higher than the Mazana passage.
The survey of the + 30 metre contour line of the Wadi Rayan proved
that there were only two outlets into the Fayûm, both on the northern
side: these two openings are only from 400-500 metres wide and their
lowest points are not below + 25 or + 26 metres.
[Sidenote: Later Government Publications by Scott Moncrieff and
Willcocks.]
In 1889 Sir C. Scott Moncrieff published[20] a further note, in which
he briefly discussed the probable cost and benefits to be derived
from the suggested reservoir, concluding that at least the project
was one worthy of being thoroughly examined.
Public-domain text, read in full here on John Shaqi.
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